Weather Alert in Wisconsin
Flood Warning issued August 12 at 10:24AM CDT until August 15 at 1:00AM CDT by NWS Milwaukee/Sullivan WI
AREAS AFFECTED: Waukesha, WI
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Wisconsin... Fox River Lower At Waukesha affecting Waukesha County. Milwaukee River Near Cedarburg affecting Ozaukee County. ...The Flood Warning continues for the following rivers in Wisconsin... Menomonee River At Menomonee Falls affecting Waukesha County. * WHAT...The river is cresting. Moderate flooding is occurring and moderate flooding is forecast. The approaches the flood of record. * WHERE...Fox River Lower at Waukesha. * WHEN...Until early Friday morning. * IMPACTS...At 8.6 feet, Water approaches the base of Bastow St bridge and Bank St bridge. Water impacts Corrina Blvd, Buckley St, W Main St and northern Bank St. Frame Park is flooded. Floodwaters are around some homes in the Bethesda Court area about one half mile south of downtown Waukesha. * ADDITIONAL DETAILS... - At 9:00 AM CDT Tuesday the stage was 8.5 feet. - Bankfull stage is 5.0 feet. - Forecast...The river is expected to fall below flood stage Thursday evening and continue falling to 4.6 feet Tuesday, August 19. - Flood stage is 6.0 feet. - Flood History...This crest compares to a previous crest of 8.9 feet on 06/09/2008. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Caution is urged when walking near riverbanks. Be especially cautious at night when it is harder to recognize the dangers of flooding. Additional information is available at www.weather.gov. The next statement will be issued this evening at 1030 PM CDT.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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